Cordilleran Section Meeting - 105th Annual Meeting (7-9 May 2009)

Paper No. 2
Presentation Time: 8:30 AM-5:30 PM

DEVELOPING THE RESAZURIN-RESORUFIN SYSTEM AS A “SMART” TRACER TO MEASURE MICROBIAL RESPIRATION AND SEDIMENT-WATER INTERACTIONS


NABELEK, Marc A., Geology, Whitman College, 345 Boyer, Walla Walla, WA 99362, HAGGERTY, Roy, Geosciences, Oregon State Univ, 104 Wilkinson Hall, Corvallis, OR 97331-5506, ZARNETSKE, Jay P., Department of Geosciences, Oregon State University, Corvallis, OR 97331, DUNNIVANT, Frank, Chemistry, Whitman College, 345 Boyer, Walla Walla, WA 99362 and KNIGHT, Thomas, Biology, Whitman College, 345 Boyer, Walla Walla, WA 99362, nabelema@whitman.edu

Water flow and microbiological activity in the hyporheic zone (stream sediment) are important to stream ecosystems. The resazurin-resorufin system can be used as a “smart” tracer to specifically measure microbiological activity and water flow through the hyporheic zone. Resazurin is a weakly fluorescent dye that undergoes a reduction reaction in the presence of aerobic bacteria to the strongly fluorescent dye, resorufin. Haggerty et al. (2008) measured resazurin reduction rates in sediment from a temperate, forested, heterotrophic stream in Catalonia, Spain, and showed that the resazurin appeared to be a feasible tracer of microbial activity and sediment-water interaction. We expanded this database by measuring resazurin reduction rates in sediment from Drift Creek, Oregon (temperate, forested/agricultural, heterotrophic) and Sycamore Creek, Arizona (desert, autotrophic) using column experiments designed to reproduce hyporheic conditions. Drift Creek had much higher resazurin reduction rates and much higher organic carbon than Sycamore Creek, suggesting that microbial biomass associated with organic content increased the rate of the resazurin-resorufin reaction.